Showing posts with label siberian archaeology. Show all posts
Showing posts with label siberian archaeology. Show all posts

Friday, 16 August 2019

Siberian Archaeology 4: Karama


Stone tools found in the Russian Altai confirm a human presence in central Asia at ca. 800,000BP. Who were these hominins and what is the evidence?  Perhaps it was Homo antecessor (pictured below from Wikimedia commons (2018))?


Karama is an open-air site in southern Siberia. It lies approximately 400km SSE of the city of Novosibirsk on the banks of the Anui River in the northwest of the Altai.
Sites in the region were first noted when 1959 with the discovery of a few flint flakes, followed by petrified bones of large animals in the Iskra Cave in the vicinity of the settlement of the same name.
It took another twenty years, for a systematic, series of excavations to begin under the direction of the Siberian archaeologist A. P. Okladnikov. In total, more than 30 caves and some open-air, sites  have now shown evidence of Palaeolithic occupation in the Anui Valley. This unique series of sites includes, Denisova Cave, Okladnikov Cave, Strashnaya Cave, Chagyrskaya Cave, Razboinichya Cave and Karama. The Karama site was discovered in 2001. Presumably this was excavation no.1, on which I have been unable to find any information. The details below refer to excavation no. 2.






The Karama site. Above: View of the site from across the valley, Shunkov (2018) and below initial stages of the excavation from Earth Chronicles (2017).


The dig in progress from Bolikhovskaya and Shunkov (2014).


Second view of the excavation progress, clearly showing the Lower Palaeolithic levels from Shunkov (2018).

On the likely hominins occupying the site and lithics discovered, Zwyns (2014) helpfully translates and summarises papers originally, in Russian: “According to Derevianko, the Altai was first colonized by small populations of Homo erectus/ergaster starting from c. 800 ka, that subsequently disappeared from the region c. 500 ka.
The site that would best represent this first wave of human occupation is Karama, along the Anuy River. The diversity of the exotic flora is said to fit with a Middle Pleistocene attribution and the RTL dates of 643 +/- 130 ka and 542 +/-  110 ka have
been obtained on the lower portion of the sequence (layers 8–14). Although the identifiable artifacts do not include handaxes, Derevianko and Shunkov tend to emphasize elements that would fit with an Acheulean attribution. The technology is described as cores on pebble blanks and flakes with subparallel dorsal pattern. The tool-kit includes various kinds of scrapers (including naturally backed examples), Clactonian notches, and choppers. More surprising is the reported presence of core-like endscrapers with abrupt retouch. Derevianko acknowledged that the first Lower Paleolithic occupation of the Altai is elusive and likely represents a short-term event.”


Lithics from the Karama site placed in the context of the recoded stratigraphy from Derevianko and Shun’kov (2008).


Lithics unearthed at Karama from Shunkov (2018). The slightly confusing, original caption reads: Hunting equipment of primitive inhabitants of the Anui Valley (left). Photo by V. Kavelin. Archaic pebble tool from the site Karama (center). A very ancient point from Karama (right). Photo by V. Kavelin.


Primitive pebble stone tool excavated at Karama from Derevyanko (2019).

On the possible assignment of the early Acheulian tools found to a Clactonian facies it is interesting to look at Stringer (2006), italics mine: “..there are further clues to the nature of the Clactonian from a site.. at Ebbsfleet. Large-scale excavations there for the Channal Tunnel Rail Link and associated engineering works since 1997 have been accompanied by archaeological investigations and, in 2003.. the skeleton of a straight-tusked elephant was found surrounded by about 100 stone tools – Clactonian tools. As at Swanscombe, pollen and other evidence suggested that this Clactonian occupation was early in the warm part of the same interglacial period (about 400,000BP). But the the association of Clactonian tools and a large mammal skeleton was very significant because it had previously been suggested that handaxes were the preferred tools for butchery at this time, yet there are none at Ebbsfleet..”
Therefore there is some precedent for lithic assemblages lacking handaxes, however the dates for the Ebbsfleet lithics are far later than those from Karama. On the other hand, the assumed habitats, climate and, faunal composition of the areas may be broadly similar. Thus an occupation resulting from an early species migration out of Africa, such as that postulated for Homo ergaster/antecessor is not out of the question. It also fits with Stringer’s idea that the hominins that made the Happisburgh footprints 850,000 years ago were Homo antecessor.
However, it was a close analysis of the palynology of the sediments that confirmed the extremely advanced age of the Karama site. Bolikhovskaya and Shunkov (2014) summarised the evidence thus:
“The composition of the autochthonous palynoflora from Karama’s three units comprises over 130 taxa of various tiers. Pollen of 45 genera and species of trees and shrubs as well as 56 species, genera, and families of herbaceous plants and subshrubs have been identified. Thirty taxa represent the spore-bearing plant group (mosses, ferns, lycopods, horsetail, and others).The palynoflora of the lower (strata 13–9) and medial (strata 8 and 7) Karama units is substantially richer than that of the earlier examined synchronous sediments at Cherny Anui and Nizhny Karakol that contained only 25 genera and species of arboreal and shrub taxa. However, according to the taxonomic composition of the dendroflora and the structure of paleophytocenoses, the periods of accumulation of these sediments were relatively close to the interglacial periods reconstructed for Karama. The pollen spectra from Karama strata 7, 8 and 10–13 contain a considerable number of elements that are non-typical of modern boreal flora (Picea sect. Omorica, Pinus sect. Strobus, Pinus cf. koraiensis, Betula sect. Costatae) and nemoral European, Far Eastern and other taxa (Juglans mandshurica, Carpinus betulus, C. cordata, C. orientalis, Ostrya sp., Quercus robur, Tilia cordata, T. amurensis, T. mandshurica, Ulmus pumila, Corylus avellana, Alnus glutinosa, A. incana, Morus sp.). Many were first recorded in the pollen spectra of the Middle Pleistocene deposits of the Anui valley. The presence of Pinus sect. Strobus, Carpinus cordata, C. orientalis, Ostrya sp., Quercus robur, Tilia cordata, T. amurensis, T. mandshurica, Alnus glutinosa, A. incana, Corylus avellana, Juglans mandshurica Carpinus betulus, Ulmus pumila, Morus  sp., etc. in strata 7, 8 and 10–13 as well as eco-coenotic features of the exotic taxa found, results of the analysis of the geographical groups of dendroflora, and other data suggest the Middle Pleistocene age of the sediments. For instance, hop hornbeam Ostrya sp. and mulberry Morus sp., belonging to the group of American-Mediterranean-Asian genera, indicate the Middle Pleistocene age of sediments in the southern Cis-Baikal and Upper Amur regions (Makhova, 1978; Grichuk, 1982). The interglacial palynofloras of Karama differ considerably from the Early Pleistocene floras of the eastern Altai, southern part of Western Siberia, and other mountainous and plain regions of Siberia and the Far East. They lack pollen grains of subtropical, broad-leaved species such as Pterocarya, Carya, Zelkova, Celtis, Ilex, Tsuga , and other exotic taxa of the pine family that are characteristic of the warm-loving Early Pleistocene floras of the named regions. This contradicts the idea that Karama dates back to the Early Pleistocene. However, some researchers argue that the Early Pleistocene age of the Karama lower unit cannot be ruled out (Zykin et al., 2005). This assumption is based on paleomagnetic testing of the entire section that yielded evidence of normal polarity as well as on the presence of two vertisols in the lower portion of the section. Previously, such soils were recorded only in Pliocene sediments of Western and Middle Siberia. This allowed V.S. Zykin and his colleagues to correlate the lower Karama strata with the Barnaul Lower Pleistocene layers, and, correspondingly, with the Olduvai subchron. However, we can hardly agree with this assumption, since the Middle Pleistocene interglacals reconstructed on the basis of the Karama pollen data differ considerably from the period of formation of the Barnaul strata in southern Western Siberia in floral, phytocenosis, and paleoclimatic characteristics. The sediments bearing the Barnaul floral remains were formed in forest-steppe and steppe zones and in a climate similar to the modern climate, while the Karama interglacial floras existed under warmer and less continental climatic conditions than today. The spore and pollen spectra of Karama indicate considerable faunal changes mirroring numerous fluctuations of plant biomes caused by climatic fluctuations over four reconstructed stages of the Brunhes event. The first interglacial recorded in the section corresponds to the accumulation period of strata 13–10 that can be correlated with MIS 19, or the Gremyachie interglacial of the Russian Plain dated to 790–760 ka BP. This period was characterized by a climate warmer than it is now and a dominance of forest-steppe and forest landscapes.”
Other commentators, also concur with this dating: from Kuzmin and Kazansky (2019): “Factual information and its interpretation regarding the geological age of the Lower Palaeolithic site of Karama (Altai Mountains, Siberia) are considered. It is demonstrated that palynological data do not allow to date this site to earlier than ca. 800 kya; archaeological data are consistent with this estimate. The viewpoint of V. S. Zykin with coauthors, according to which the age of Karama is ca. 1.95-1.77 mya, finds no support in the light of the available geological and paleomagnetic evidence. The so-called “Karama suite” of the Upper Pliocene of Altai Mountains in reality does not exist. For the time being there are no reliable data indicating than the initial peopling of Siberia took place prior to ca. 1 mya.”

References
Bolikhovskaya, N.S. and Shunkov, M.V., 2014. Pleistocene environments of northwestern Altai: Vegetation and climate. Archaeology, Ethnology and Anthropology of Eurasia, 42(2), pp.2-17.
Derevianko, A. P. and M. V. Shun’kov (2008) Early Paleolithic of Altai in Early Paleolithic Of Eurasia: New Discoveries, International Conference Program and Abstracts Krasnodar – Temriuk, 1–6 September 2008 S. A. Vasil’ev, A. P. Derevianko, G. G. Matishov, Kh. A. Amirkhanov, V. E. Shchelinsky, A. A. Velichko, G. I. Medvedev, L. B. Vishnyatsky, S. A. Kulakov, V. V. Titov eds.
Derevyanko A.P. (2019). Science First Hand “Where has Homo sapiens come from” from: https://scfh.ru/en/papers/where-has-homo-sapiens-come-from/ accessed 17.08.19
Earth Chronicles (2017) “There are confirmations that people appeared in Siberia 800 thousand years ago” at: http://earth-chronicles.com/science/there-are-confirmations-that-people-appeared-in-siberia-800-thousand-years-ago.html accessed 14.08.19
Kuzmin, V. and Y. Kazansky (2019). Chronology of the Lower Palaeolithic Site of Karama (Gorny Altai): Facts and Problems. Stratum plus. 2019. No1 online at
Shunkov, M.V. (2018). Science First Hand, “The Golden Section of the Anui” from https://scfh.ru/en/papers/the-golden-section-of-anui/ accessed 14.08.19
Stringer, C., 2007. Homo Britannicus: The incredible story of human life in Britain. Penguin UK.
Wikipedia commons (2018) https://commons.wikimedia.org/wiki/File:Homo-Antecessor.jpeg accessed 17.08.19

Monday, 8 April 2019

First Denisovan Cranial fragments discovered.

I know news of this discovery has been around for a while but I missed it until a report on the 88th Annual Meeting of the American Association of Physical Anthropologists came to my attention.

Parietal fragments, discovered back in 2016 were, at last, confirmed by 
DNA analysis to be that of a Denisovan. These were the subject of a Podium presentation. Here's the abstract from the conference:

A parietal fragment from Denisova cave (see here) Viola, B.T. et al. (2019)
The Denisovans are an Asian sister group of Neanderthals, originally described based on ancient DNA from a phalanx fragment from Denisova Cave (Altai Mountains, Russian Federation). Since then, three teeth found in the cave have been identified from this group. Genetic data indicates that this population contributed genes to modern humans across large parts of Asia and in Melanesia, but currently, no fossils from outside Denisova Cave have been clearly attributed to Denisovans. One reason for this is that the extremely limited morphological evidence hampers comparisons. A newly discovered parietal fragment, Denisova 13, attributed to the Denisovans based on its mtDNA, gives us a first glimpse at the Denisovan cranial morphology.
Denisova 13 derives from the South Gallery of Denisova cave, although due to a collapse of the section, its stratigraphic position is not secure. Based on its preservation and the accompanying sediments we tentatively attribute it to Layer 22.The specimen consists of two adjoining fragments of the posterior half of the left parietal, extending about 78 mm laterally of lambda, and about 51 mm anteriorly, preserving portions of both the sagittal and lambdoid sutures.
We compare Denisova 13 to a large sample of recent and fossil modern humans, Neanderthals and Middle Pleistocene Homo, using geometric morphometrics based on three-dimensional landmarks and sliding semilandmarks collected on computed-tomographic scans and surface scans.
We will discuss the implications of these comparisons to our understanding of Middle and Late Pleistocene hominins in Asia.
At a press conference Viola is quoted by the Science Alert (2019), as saying: "It's very nice that we finally have fragments like this," says Viola. "It's not a full skull, but it's a piece of a skull. It gives us more. Compared to the finger and the teeth, it's nice to have." But, he adds, it's hardly a full skeleton.
"We're always greedy," he laughs. "We want more."
A report by Science News (2019) gave a little more detail: "Viola, of the University of Toronto, and his colleagues compared a digital reconstruction of the skull fragment with corresponding parts of 112 present-day human skulls and 30 Stone Age Homo skulls, including Homo sapiens and Neandertals. The Denisovan find didn’t fit neatly into any previously known Homo species. Some features linked the Denisovan fossil to Neandertals and to a 430,000-year old Spanish Homo species that had Denisovan ancestry. The Denisovan skull fragment is surprisingly thick, more like cranial bones of Stone Age Homo erectus, Viola said."


Scientist at Denisova Cave. Second left Katherina Douka of the Max Planck Institute, part of the team that successfully extracted DNA from the parietal fragments. From NY Times (2019).

References:
Science News (2019). "The first known fossil of a Denisovan skull has been found in a Siberian cave" at https://www.sciencenews.org/article/first-fossil-denisovan-skull-cave-siberia accessed 09.04.19
Science Alert (2019). "Scientists Just Confirmed The Discovery of The First Ever Denisovan Skull Fragments" at: https://www.sciencealert.com/first-confirmed-denisovan-skull-piece-found accessed 09.04.19

New York Times (2019). "High Ceilings and a Lovely View: Denisova Cave Was Home to a Lost Branch of Humanity” at: https://www.nytimes.com/2019/01/30/science/neanderthals-denisovans-humans.html  accessed  09.04.19



Sunday, 28 January 2018

Siberian Archaeology 3: Ulalinka


The settlement of Ulalinka or Улалинка, in Russian (co-ordinates 51°57'20.0"N 85°58'18.6"E) was discovered in 1961 by Okladnikov, it lies partly under the old city cemetery on the south-eastern outskirts of Gorno-Altaisk.

The first, source I could find regarding the manner of his discovery was Anatolevna (2013). She quotes the author himself: “In his book "The High Hill" Okladnikov wrote: "In 1961, during the local lore conference, the instinct of a hunter for primitive man led me and ethnographer Tashchakov to this hill, forced me to cross a small mountain river Ulalinka and climb up a steep hillside strewn with stones."
Reading between the lines, I think we can conclude that local people directed him to the site and upon inspection he found stone tools eroded out of the slope.
This, is more or less, confirmed by a second source, Gavrilov (2012), who gives a little more detail about the site’s discovery: “In 1961, the famous Soviet archaeologist and historian AI Okladnikov came to Gorno-Altaisk for several days. In his spare time, after a long-established habit, the scientist began to search for new monuments of antiquity in the vicinity of the city. His attention was drawn to the left bank of the Ulalinka River near the old city cemetery. Here the river washed away a high terrace, in the upper layers of which, before 1961, a parking lot was found for people who lived in the late Paleolithic era (the end of the Stone Age).
At the bottom of the terrace L.P. Okladnikov found several yellow-hazel, quartz with traces of rough treatment by their man. It was these findings that struck him with his closeness in the processing technique to the pebble tools of the Punjab (India) and distant Africa, i.e. the oldest known tools of man's labour, which preceded the tame chisels of the lower (early) Palaeolithic.”
However, when Okladnikov reported his finds and suggested great age for them his colleagues were sceptical. They pointed out that two questions needed answering about the site, before the tools could be accepted as truly ancient. These were:
1.Do the pebble tools belong to the lower, ancient layers of the terrace or have they been transported there, perhaps by water? 
2. If so, then what is the age of these layers?
Therefore, a full excavation was required. This had to wait for eight long years before it could be organised. Garilov (ibid.) continues:
“In June 1969 a group of researchers from the Institute of the Institute of Physics and Technology of the Siberian Branch of the USSR Academy of Sciences, headed by AP Okladnikov (including the associate professor of the history department of the Barnaul Pedagogical Institute, Umansky Aleksey Pavlovich, and the student-historian BGPI V. Mamaykin) laid an exploratory dig on the slope terraces. During excavations, in addition to a series of stone tools of labor, bones of some fossil animals were found, in particular a tusk of an elephant or a mammoth.
In July of the same year, students-historians BGPI on behalf of AP Okladnikov made a step-by-step cleansing of the slope of the terrace. These were the first excavations in the Ulalinsky parking lot.
During the excavation in 1969, more than 500 pebble tools were found, as well as bones of small rodents.
Part of the slope was cleared from the base to the top so that geologists could make a complete picture of the structure of the terrace and, consequently, solve the question of its origin and the age of the layer in which primitive tools of labour were discovered.
I must say that before the excavations in 1969, geologists were also not unanimous in explaining the origin of the terrace and differently dated the time of its formation. Thanks to excavations in 1969, the structure of the terrace was traced on a wide front.
 After studying it in the autumn of 1969, geologists - Corresponding Member of the USSR Academy of Sciences VN Saks and candidate of geological sciences S. L. Troitsky came to the conclusion that the terrace (120-100 thousand years ago) was very old. This time was also dated the layer containing pebble tools.
But the excavations of 1969 did not give a clear answer to the question of how these weapons fell into the ancient layer: whether they were left by the people who lived then (and, therefore, are very ancient) or in fact, slid from the upper layer to the lower one (and then belong to later time).  This problem could only be solved after excavation at the top of the terrace.”
Okladnikov (1982), states that he opened a pit on top of the terrace and dug down over 5m. Garilov (ibid.) concludes:
“In the summer of 1970 excavations at Ulalinka were continued. In the lower part of the cover layer, that is, at a depth of two meters [note the depth discrepancy with Okladnikov’s paper], dozens of the oldest pebble tools were found on the entire area of ​​the site. They proved that there is no question of any sliding of the found tools from the upper layer, that they really, belonged to the lower layer, that is, their grey antiquity was proved. This was confirmed by archaeological materials, from which the tools of labour were made, and the technique of production, and their types.”


Ulalinka excavation in 1969, from the Assa at the Megalithic Portal (2016)




Okladnikov at Ulalinka in 1979, the year before his death. Original caption reads: The excavation site; journalist B. Alushkin, academician A. Okladnikov (center) and geologist V. Mylnikov at Ulalinsky parking lot (1979). Source: Badanova (2015).

Anatolevna (ibid.), a local resident of Gorno-Altaisk, describes the site as it is today:

“The site was named after the Ulala River. It is located near the old cemetery on the left bank of the taiga river Ulala”.. “Poplar planting in the old cemetery serves as fencing around the site. Garages, sheds, residential buildings are built under the very precipice.”
Of the finds made by Okladnikov she states “more than 600 samples of primitive tools from quartz were extracted.”

According to the ООПТ России (Protected Areas of Russia) website (2018) the site’s importance was first recognised by a decision of the Altai Territory Council of People's Deputies in 1978 in a document entitled "On the Approval of Natural Monuments of the Gorno-Altai Autonomous Region". In 1996 it received national recognition as an ‘object of historical and cultural heritage of all-Russian significance’, by presidential decree. The site, however, was largely ignored and left unprotected until 2012. Then, the Altai Republic, prosecutor's office stepped in. It was reported, by Federal Press (2012) that they demanded that the federal agency for managing state property and the Ministry of Culture take measures to preserve the cultural heritage site, Ulalinsky.
According to, Badanova (2015), action seems to have been taken: the site now has a sign-board, and improvised open-air museum based in a yurt, which also serves as a ticket booth. A museum complex is also planned.


Recent images of Ulalinka:




Ulalinka site from the south, showing the creeping development threatening the site. Source: Wikipedia commons (2016).


New sign board at Ulalinka. Source Badanova (2015)

Ulalinka site plan from the Protected Areas of Russia, Natural Monument Passport. PDF download from ООПТ России (Protected Areas of Russia) website (2018). Original caption reads: Fig 1 Site plan of the Ulalinka Natural Monument.


View of Ulalinka from the north(?). Source: Assa at the Megalithic Portal (2016).

The only published paper on it is that by its excavators A.P. Okladnikov, A.P. and G.A Pospelova (1982).


In their own words:
“The Ulalinka site, discovered in 1961, is located on the right tributary of the Maima River, on the left bank of the Ulalinka below the cemetery of Gorno-Altaisk. The site is situated in the submeridional fault [meaning a fault in an almost north-south direction]. Zone separating the Biisk-Katun and Kiam synclinoria. It is located on the edge of Iolgo Range, which is composed of flint limestones, quartzites and other rocks of late Proterozoic age [ended 542Mya]. These rocks are occur at a depth of 12m below the Ulalinka River level and are overlain by Neogene and Pliocene-Quaternary sediments.”
In this section, the authors are trying to put the cultural levels in context to show what age they are.
“The Ulalinka section, in which two distinct cultural levels were found, was exposed on the slope of the and in a pit dug into the hilltop to a depth of 5.8m. The section’s strata differ in genesis and form three informal units”
“In one of the pit’s walls the section was as follows: (1) modern, black, soil 0.70m; (2) greyish-brown loam with worm tunnels and roots of vegetation, 0.3m; (3) loessy light-grey loam with columnar parting and lime nodules, 0.3m and (4) loessy light-brown loam with lime nodules 0.4m. These four layers comprise a loam unit of typical late-Quarternary appearance, an identification confirmed by finds of molluscs. The first cultural level is confined to the lower part of this loam unit. The section proceeds with (5) lumpy brown clay, 0.45m; (6) compact brown clay with iron hydrates, 0.5m; and (7) yellowish-brown clay with some crushed stone, 0.45m. These layers comprise a middle clay unit of which the general appearance indicates a much earlier Quarternary age than that of the loam unit. Finally, the section includes (8) a boulder-pebble horizon with gravel, crushed stone, unsorted fragments, flint limestones, porphyrites and diabases associated or stained with yellow-brown ochre clay, 0.6m; (9) yellow-brown ochre compact clay with rhythmically alternating thin inclusions of white clay, 0.35m; (10) bright-yellow clay, 0.25m; and (11) crushed stone and pebbles of quartzite and limestones, 1.5m. Layer 8 is the second main cultural level of the section. These four layers comprise the lower clayey unit, the rocks of which are typical of the Pliocene Altai foothills in their lithology and multi-coloured character. Until this discovery, Palaeolithic artifacts had not been found in Siberia under the thick cover of loessy loams in rough sediments with pebbles and crushed stone. The upper cultural level is a typical assemblage of Upper Palaeolithic implements, including a few flakes, some fragments of prismatic core, a point, and a small scraper with semi-lunar blade made of obsidian. These tools and many others from similar sites can be attributed an age younger than the Sartan glaciation (less than 25,000 years).”
The main cultural level of the section, associated with the boulder-pebble horizon, differs from the upper one and from all other known Palaeolithic sites in Siberia principally in the strikingly archaic shapes of the tools and their primitive technology. The tools were made almost entirely from pebbles of yellowish-white quartzite, whole or split in half, and sometimes from pebbles of obsidian and quartzite fragments. The finds include choppers, chopping tools, scrapers, a peculiar pebble core and tools with a spoutlike curved projection that might have served as cutting instruments. All these tools are nearly untreated pebbles, only slightly retouched (fig 1). All the artifacts are amorphous. They may sometimes have served as cutting tools, sometimes as scrapers, sometimes both functions at once. Their primitive diversity seems to reflect the pursuit of a useful and stable shape. The stone inventory and the techniques of manufacture are so primitive and peculiar that they cannot be classified in the framework of the classic Lower Palaeolithic typology. The nomenclature of the Western European schemes cannot be applied to them.”

A closer look at the stone tools
In their paper Okladnikov and Pospelova (1982) sparsely illustrate their collected lithics:



Ulalinka primitive stone tools from Okladnikov and Pospelova (1982). Original caption reads: Fig.1. Stone inventory Ulalinka, lower horizon. 1, pebble with marks of percussion along the longitudinal edge; 2, tool with re-touched projections; 3, pebble chopping tool; 4 scraper-like tool; 5, pebble core.

Ulalinka lithics from Russia’s Archaeological Web Museum (1999). Original caption reads:
According to the latest archaeological finds, ancestors of present man lived in Gorny Altai many hundred thousand years ago. Ulalinka which lies within the limits of today's Gorno-Altaisk, is the most ancient settlement of primitive man. During the excavation of the Ulalinka site some primitive stone tools were found. The fire technique, that is the heating and quick cooling of stones, was used when making the tools. Ulalinka's finds are dated within the limits of the lower Palaeolithic period - from 150000 BC to 1.5 million years.



Stone tools, purportedly, from Ulalinka from Anatolevna (2013). No source is given and no caption. Provenance unknown. Although, I must say, they do have a marked similarity with those pictured on the Russian Archaeological Web Museum website.


Ulalinka lithics from the Guide to the Republic of Altai website (2014). Source not stated and no caption. Left hand specimens and hafted point possibly from the upper cultural levels, whilst the black and white line drawings are much more in keeping with the other sets of lithic tools above. However, the largest flaked tool at middle, with the black bar on it is from Fig. 3 of Derevianko et al. (2005) and is, actually from Kara-Bom!

Firstly, I must say, I find the typification of the stone tools by Okladnikov and Pospelova as “nearly untreated pebbles, only slightly retouched”, quite self-serving. By emphasising their primitive aspects and giving a scant description of their more advanced features, they are leading the reader to their preferred conclusion: these tools are extremely old.

Secondly their statement that “The stone inventory and the techniques of manufacture are so primitive and peculiar that they cannot be classified in the framework of the classic Lower Palaeolithic typology. The nomenclature of the Western European schemes cannot be applied to them.”, seems to ignore parallels with other, ancient, tool traditions from India and Africa that the authors must have been aware of, especially considering his own stated familiarity with them.

Looking at what Okladnikov’s team found, if the tools shown on Russia’s Archaeological Web Museum are from Ulalinka, it seems to me, that even an untrained amateur can attempt an explanation their manufacture and hence make a stab at their possible age.

Studying the images of these tools closely I was struck by their close resemblance to a technique used on pebble raw materials that I have seen before. To me, it seems, that they may have been produced by bi-polar lithic reduction in addition to the use of, fire as stated by Okladnikov.

Comparing Okladnikov’s Fig 1-4 and the specimen at right from Russia’s Archaeological Web Museum with a schematic drawing of this technique from the Lithic Reduction article on Wikipedia (2017), the similarities are striking:



I was extremely puzzled by this discrepancy, and thus sought out commentaries on early lithics from central Asia and Siberia to find out what other authors professional opinions were, about the lithics from Ulalinka.

From Shunkov (2005):
Until recently, archaeological materials from the Ulalinka site have been the only evidence of human occupation of the Altai during the Lower Paleolithic. Stone tools
made of split quartzite pebbles were recovered from multi-coloured soft sediments, which have been dated to the Middle Pleistocene and Upper Pliocene (Derevianko et al. 1998a). An abundant collection of quartzite rocks recovered from the lowermost layers of Ulalinka comprise such indisputable artifacts as pebbles bearing evidence of core preparation and negative scars of irregular detachment of amorphous flakes. Furthermore, massive pebbles trimmed along the long axes to form chopper/chopping tools, scraper-like tools worked on flat pebbles with a natural back and the cutting edge formed through stepped retouch, and pebble tools with a spur-like ovoid protruding part were recovered (Okladnikov 1972).

Note the reference to Okladnikov (1972). This is the original paper on the lithic tools, that caused the controversy in Russian archaeology. The problem was that an extremely ancient age was being claimed for the Ulalinka based primarily on the typification of the tools. Some other Russian archaeologists strongly disputed this.
Note also the much greater detail given. First, let us assume, for the sake of argument, that Shunkov (2005) gives an accurate translation of the Okladnikov (1972) text. Reading this second account, it is clear the lithic assemblage was far more diverse and advanced in terms of the techniques of tool production used than the scant description given by the author in the only English language paper written about the site!

So, let us look at the tow descriptions side by side:

Given these discrepancies I felt I had to delve into the techniques used in the production of tools from pebbles, to see if any research carried out since Okladnikov’s time could shed light on these varying descriptions.


One excellent source I discovered was Van der Drift (2009).
Van der Drift, is an amateur scientist from the Netherlands with his own website, espousing a very nationalistic view of the first waves of migration into his country, by ancient hominins. His, particular, interest lies in, the lithics found there, and their categorisation. Many specimens he, and others have collected over three decades, do not fit the received/orthodox view of the first colonisation of the region by Neanderthals. His view is that a much earlier, migration must have occurred. He bases his theory on the types lithics found in this part of Europe. Controversially, he believes, and has stated, in a number of web-based publications that, Homo erectus/Homo antecessor/Homo heidelbergensis was present and making stone tools, in his country, at an extremely remote epoch, of ca. 800,000 to 1Mya.
Why use his paper? Well his lithic samples, and his detailed explanation of the lithic techniques, used to produce them, bear a striking resemblance to some of the lithic inventory from Ulalinka.

In his paper, he goes into great detail about how, he believes, ancient hominins, used the bipolar technique on ovoid pebbles or river cobbles to produce usable stone tools.

I will highlight how his research matches the lithics from Ulalinka.

Firstly, he states that, the bipolar technique is used on pebbles or river cobbles of a fine grained, and isotropic structure, such as quartz, quartzite and especially flint. This is exactly the material used at Ulalinka.
Next he goes into great, detail about how freehand flaking produces usable flakes, with the fracture will always following the outlines of the core. In particular, he states that the flakes produced, take on a well characterised, defined, conchoidal shape.
He further states: “This basic understanding of freehand flaking, teaches us that freehand flaking does have its limitations. It is for instance impossible to peel off flakes from a round, core (i.e. a river pebble) because it has no striking plane, no reduction face, no edge or rib. And a freehand blow directed to the centre will be too weak to break the core, at its best it will produce a dead-end cone. That could certainly prove to be a great problem for early hominids living on the edge of a river, when all they find at the river banks are rounded pebbles.”
He then, goes on to show that the forces exerted, on rounded river cobbles, by the freehand flaking method are insufficient to break these cobbles. Furthermore, he shows that the use of a hammerstone AND an anvil – the bipolar technique – are the only method by which useable core could be prepared for further reduction.
Put simply, the application of the bipolar technique is the only way in which river cobbles can become prepared cores.
Putting these observations into the context of how ancient hominins actually lived Van der Drift (2009), says “The advantage of the freehand technique is that it produces blades and flakes in an effective, reliable, controlled way. Because of the control that it gives, it was the technique of choice for most hominids with access to large isotropic stones. But in the palaeolithic many hominid groups in lowland river delta areas could not find large isotropic stones. Instead these hominid groups had to rely on pebbles and bipolar techniques. The industries that these hominids produced (for instance Vértesszöllös) are called pebble-tool-cultures due to the obvious use of pebbles as raw material. But the role of the bipolar techniques in pebble-tool-cultures has hardly been investigated and often denied. We should get a better understanding of the possibilities that bipolar techniques offer, few archaeologists have even recognised that bipolar techniques offer choices. In order to understand Pebble tool cultures and related industries we must study the options that the bipolar techniques offered.

His Fig. 5 shows the results of different angles of hammer impact on pebbles:


Van der Drift (2009) Fig. 5. Original caption reads: Figure 5: bipolar techniques A and B straight, C oblique, D and E retouching, F contre coupe, G notching


Exploring how different hammer-stone striking angles, affect the way pebbles shattering when the bipolar technique is used he defines two modes of reduction: straight bipolar technique and oblique bipolar technique, each resulting in different, shaped prepared core.
Continuing, his argument, Van der Drift (2009) makes a crucial point: “It is difficult to distinguish between oblique bipolar flakes and freehand flakes. Oblique bipolar flakes never show any double contact points or double ripple patterns. And smaller differences (i.e. different angle, striking plane, curvature, bulb formation, bulbar scar location) are easily overlooked. This explains why for instance László Vértes mistakingly thought that “No traces indicative of a bipolar technique have been observed.” in Vértesszöllös. Just like any freehand flake does, flakes made in oblique bipolar technique show only one contact point, a sharp edge at the opposite side and they have a nearly conchoidal shape.

This is the main point of his entire chain of reasoning: tools made on river cobbles/pebbles have been worked by the bipolar reduction technique and that the results of the use of it, by hominins on the Eurasian continent, remain, largely unrecognised.

Lastly he examines bipolar retouching of these ‘prepared core’:

It is possible to start out with a rounded pebble, break it open with the nutcracker technique and as the broken pieces have striking planes and reduction faces, you can
than proceed using freehand techniques. This is actually what D. Mania proposes for Bilzingsleben. I do not believe that this is what happened. In Bilzingsleben there might certainly have been some opportunistic freehand flaking, just like in other bipolar traditions. But the majority of the further shaping and retouching of the artifacts was done in bipolar technique, as shown in figure 5D and 5E. This is proven by the tool shapes (discussed in my film “the bipolar toolkit concept”) and the signals discussed
in chapter 3. The first reason for bipolar retouching is that anvils proved to be very helpful in working steep edges, it is often still very difficult to shape split pebbles using freehand techniques. But this is not the only reason to use oblique bipolar percussion in shaping and retouching implements, this choice was also greatly influenced by habit, tradition and culture.

Lastly Van der Drift (2009), expresses his opinion on the development of the pebble tool culture in the middle Pleistocene:
“ ..the repeated and habitual use of bipolar techniques in the initial shaping of pebbles must have trained the hominid mind in understanding the consequences of bipolar reduction. Anvil use was a habit in some traditions! And it goes much further because each step of the production line was part of the integral tradition, from the gathering of
pebbles as raw material on the banks of a stream to the next step of bipolar breaking and the following step of bipolar shaping to the final step of the application of the tools. Groups using the freehand toolkit concept had the habit of using freehand flaking on good raw material (often found on open planes and in mountains), most often with the intent of using bifacial reduction to make handaxes (long cutting tools) that were meant for meat and hides processing (from large grazers in open landscapes).
Groups using the bipolar toolkit concept often lived where good raw material was difficult to find such as forests and river deltas. They had the habit of using bipolar reduction to make choppers, steep scrapers, deep notches and related tools. In the early Oldowan the choppers were used directly for food processing and this meant that the invention of long cutting tools was an improvement and the decisive step towards the Acheulean.
But in the middle Pleistocene bipolar traditions in Europe and Asia, the steep scrapers and notches and related tools were meant for wood and bone processing. The combination of stone and wood and bone tools were used to process food. So the bipolar toolkit traditions had developed a completely different concept of suitable raw material, a completely different concept of tool-shapes and a completely different concept of tool-use.  The group or microband of hominids had a completely different concept in their collective memory than the freehand groups. It was not the simple cracking open of small pebbles (Mania called this Zertrümmern) but it is this complete concept that ensured survival of the group.

Van der Drift (2009), also illustrates some of the lithics he believes were produced by bipolar technique. Interestingly, these include some retouched specimens very reminiscent of those from Ulalinka (compare the right-hand specimen from them Russia’s Archaeological Web Museum (1999) and the bottom left specimen from Okladnikov (1982)) :

Pebble tools, with retouch, produced by bipolar technique from Van der Drift (2009). Original caption reads: BIPOLAR RETOUCHING Tayac-points are converging denticulates and are most often small (scale 5 cm.) and triangular in cross-section, they should not be compared to handaxes which are smooth edged bifacial large cutting tools.


Reflecting back on the lithic tools found at Ulalinka, it seems more than probable that many of the tools found in the lowest cultural level were produced by the bipolar technique.
The tools these hominins, produced may instead of being extremely ancient, result from an expedient use of the raw materials found in the region. The absence of blades and points, whilst seeming to indicate a truly ancient origin for the tools found, may, in fact indicate that the tool-makers were simply from a different tool tradition, which used bone points as hunting weaponry and stone tools for hide and wood working. Thus their age may NOT be as ancient as Okladnikov (1982) believed.
Let us look now at the dating techniques used by Okladnikov to see if the evidence he presented is strong enough to support his ‘late Pliocene’ age for the site. He says:

The archaeological data alone were insufficient to estimate the age of the tools. Geological, paleogeographical, and paleontological methods were also used, though they did not yield a common result. Some scholars, noting the relatively low elevation of the site, thought it no older than 40,000 years, while others dated it to the middle Pleistocene (Okladnikov 1964, 1972; Gaiduk 1968; Ceitlin 1979) and still others to the early Pleistocene on the basis of the geological conditions (Adamenko 1970). A further group of scholars assigned it to the late Pliocene on the basis of the paleogeographical environment and the lithology of the cultural level (Okladnikov and Ragozin 1978a and b). The paleomagnetic method was employed to help solve this complicated and very important problem (Pospelova, Gnibidenko, and Okladnikov 1980; Okladnikov Pospelova, and Gnibidenko 1981)

The Paleomagnetic method was used to date the stratigraphic column at Ulalinka and, in particular the clay layer in which the oldest stone tools were found. This method relies on the fact that lava, clay, lake and ocean sediments all contain microscopic iron particles. When lava and clay are heated, or lake and ocean sediments settle through the water, they acquire a magnetization parallel to the Earth's magnetic field. After they cool or settle, they maintain this magnetization, unless they are reheated or disturbed. The remanent magnetization, that is the magnetisation of the rocks or sediments, from the time they were laid down can be found by the application of suitable laboratory techniques.

The description of the number of samples taken from the various stratigraphic layers; their special distribution and the care taken in recording their orientation seems sufficiently detailed and to my, admittedly, amateur eye to be professional enough to provide reliable data.
The temporal “cleaning” techniques applied to the samples in the laboratory; both Alternating Field Demagnetization and Thermal Demagnetization, also seem sufficient to remove any of the later, secondary magnetizations and reveal the characteristic Natural Remanent Magnetization (NRM) component from when the sediment in which the tools were initially laid down.

In summary Okladnikov and Pospelova (1982) found two very minor Paleomagnetic reversals in the stratigraphic column and a major Paleomagnetic reversal in the clays of the lower cultural level.
They state:
Thus a summary paleomagnetic section of Ulalinka was compiled after a set of magnetic cleanings of rocks, the result for three paleomagnetic sections complementing each other. It consists of two paleomagnetic zones. The sediments of the upper unit comprise a normal paleomagnetic zone that can be compared unambiguously with part of the Brunhes polarity epoch and the sediments of the lower unit represent a reversed zone that can be attributed with nearly equal probability to part of the Matuyama polarity epoch or an older reversal event Its age is quite definitively older than 690,000 years.

The authors go on to note that if the Brunhes-Matuyama boundary is considered the dividing line between the Pliocene and the Pleistocene then the site with its lithic implements older that this boundary is a late Pliocene one.

Since 2009 the Pliocene-Pleistocene boundary has been re-allocated to 2.588 ± 0.005 Ma. The Brunhes-Matuyama boundary reversal is now dated, based on further research to 781,000 years ago. This date has been set as the boundary between, the lower and middle Pleistocene.
The Ulalinka site, based on Okladnikov and Pospelova (1982) would thus be of lower Pleistocene age.

Commenting on the dating of the site Shunkov (2005) says: “The available palaeomagnetic and radiothermoluminescence (RTL) dates suggest attribution of the lowermost layers at Ulalinka to a wide chronological range of c. 300 - 400 ka to 1.5 mya (Okladnikov et al. 1985). The lower chronological boundary seems doubtful, whereas the upper boundary is reliable, supporting the age estimates of the Ulalinka site as older than 300 ka.

The nearby Karama site, with comparable lithic tools in its lowest cultural level, is provisionally dated to the final Lower Pleistocene. The two sites may therefore be comparable in age and presumably, were occupied by the same hominins.

Conclusions
  • The Ulalinka site can be dated reliably to older than ca. 300,000 years old. 
  • The tools found appeared of ancient derivation due to their primitive form. This fact swayed Okladnikov to posit that they were extremely old, when in fact the hominins who manufactured them were simply making expedient use of local material, a material necessitates the use of the bipolar technique. The tools may therefore be of any age.
  • If the Paleomagnetic data collected by Okladnikov and Pospelova (1982) are correct, then the site is older the Brunhes-Matuyama boundary reversal and is thus of final lower Pleistocene era and somewhat earlier than 781,000 years old
  • The claim that the site is from an even earlier date of ca. 1.5Mya has only slight evidence and unlikely to be correct
  • Further research is required to establish, the exact age of Ulalinka and whether is truly the oldest site of human occupation in Siberia


References

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